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Published byAngela Patrick Modified over 6 years ago
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Determining the Relative and Absolute Age of Map Units
GEOL 3000 Geologic Maps Determining the Relative and Absolute Age of Map Units
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Relative Age Dating - Superposition
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Up isn’t always Younging
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Up Indicators Graded Bedding Pillowed Lavas
Amygdaloidal Zones in Lavas Cross-bedding Ripple Marks
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Sedimentary Facies – Time Trangressive Units
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Paleogeography of Middle Laurentia in the Paleozoic
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Advanced Transgression
Regression
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Paleozoic Formations of the Upper Midwest
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Principles of Faunal Succession and Faunal Assemblage
Index Fossils - Widespread distribution - Restricted, known time of existence - Common to many environments
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The Jordan Sandstone Unconformity Missing Fossils
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Gaps in the Geological Record Unconformities
Siccar Point, Scotland “The mind seemed to grow giddy looking so far into the abyss of time” John Playfair – Illustrations of Huttonian Theory (1809)
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Creating Unconformities
Nonconformity Angular Unconformity Grand Canyon Stratigraphy Disconformity
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Unconformities or Pinch-outs?
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Gaps in the Minnesota Timescale
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Regional Correlation of Units Piecing the Rock Record Together
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Relative Time for Intrusive Igneous Rocks Principle of Cross-cutting Relationships
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Global Time Markers Volcanic Ash Eruptions
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Global Time Markers Meteor Impacts
K-T Boundary mudstone-impact layer coal K-T impact site
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The First Major Extinction Event ??
The Ga Sudbury Impact The First Major Extinction Event ??
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Global Time Markers Magnetic Reversals
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Global Time Markers Climate Change
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Absolute Age Determinations Radiometric Dating
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Radioactive Isotopes
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Radioactive Decay
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Radioactive Decay Half-life
Zircon ZrSiO4 U substitutes for Zr, but Pb does not.
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Rb-Sr Dating of a Granite
87Rb 87Sr; 86Sr is stable Rb – chemically substitutes for K Sr – chemically substitutes for Ca Isochron t=2 t=1 87Sr/86Sr Metamorphism at t=1 87Sr/86Sr°(m) t=0 87Sr/86Sr° 87Rb/86Sr Ca-plagioclase Granite whole rock K-feldspar Biotite (K-rich)
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